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1.
《Coastal Engineering》2004,51(10):967-990
Inlet relocation is a coastal management tool that, when applied to a migrating inlet, involves the artificial opening of a new tidal inlet along the historic migration path of the inlet. The old inlet is then artificially closed, or it is left open and will eventually close if the new inlet captures the entire tidal prism. Two inlets were relocated in such a manner in Southern Portugal and then were the subject of a monitoring program that included the acquisition of quantitative (topo-bathymetric surveys) data. Data was acquired for 4 years after the relocation at one of the inlets (Ancão Inlet) and for 2 years at the other (Fuzeta Inlet). The data obtained from the monitoring program were analysed together with the wave climate and then compared with historical information on the natural inlets, in order to assess the degree of success of the relocation actions. One of the relocations studied, Ancão Inlet, was considered to be successful even though an initial unexpected behaviour produced some material damage to property. On the contrary, the relocation of Fuzeta Inlet did not have the expected results, and the new inlet was affected by the same problems as the old one.It was found that the most important factor for a relocation action to succeed is the correct choice of the opening location. A theoretical procedure to enhance the possibilities of relocation success is suggested. (1) Hydrodynamic studies are needed in order to determine if the present conditions are similar to the historical ones. (2) The position for the inlet opening is chosen according to the hydrodynamic conditions, but there are other factors to be taken into account, i.e., the historical migration paths and typical inlet width of the natural inlet; the hydrodynamics of the backbarrier; the morphology of the backbarrier and, for multi-inlet barrier island systems, the proximity to adjacent inlets. (3) Once the position is chosen, environmental impact studies should be made in order to assess the risk of the relocation for the ecosystems of the area. Only if the environmental impact studies are favourable should a relocation action be performed. 相似文献
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以蛇鲻Saurida elongata内脏为原料,将蛇鲻胃经组织捣碎,硫酸铵分级沉淀,HitrapTMQ FF离子交换层析,Sephadex G-100凝胶过滤层析,得到胃蛋白酶纯品。经SDS-PAGE显示为单一条带,酶的分子量为37.7kDa,测得其最适温度为45℃,最适pH为2.2,酶的热稳定性很好,在40℃及以下温度处理3h酶活力没有任何变化,酶在pH 1—10以下都比较稳定,在强碱性条件下不稳定。EDTA和Trypsin inhibitor对该酶都没有明显的抑制作用,PMSF和Pepstatin A能完全抑制胃蛋白酶的活性。Ca2 、Mn2 、Mg2 、Ba2 对该酶影响不大,Hg2 对酶有较弱的抑制作用,而Zn2 、Cu2 、Fe3 对酶的抑制作用较强。 相似文献
3.
利用贝类废弃物制造水解动物蛋白 总被引：2，自引：0，他引：2
以扇贝加工废弃物—扇贝边为原料 ,采用枯草杆菌蛋白酶、胰蛋白酶、Flavourzyme对其进行深度水解 ;然后应用超滤技术对酶解液进行分离 ,除去未水解的蛋白质、细菌、微细的颗粒等物质 ,得到富含氨基酸和小分子肽的超滤透过液 ;再应用反渗透技术进行预浓缩 ,以除去其中过多水分 ;最后 ,对该浓缩液进行减压浓缩或喷雾干燥 ,即得到浓液状或粉状的水解动物蛋白产品。其中 ,粉状产品的粗蛋白含量为 6 6 .88% ,氨基酸态氮含量为 6 .96 % ,氨基酸态氮 /总氮 6 5 .0 5 % ,均优于国外同类产品 相似文献
4.
A. Oliveira F. Rocha A. Rodrigues J. Jouanneau A. Dias O. Weber C. Gomes 《Progress in Oceanography》2002,52(2-4)
The Northern Iberian margin is a typical example of a continental margin subjected to seasonal highly energetic regime (waves and tides) and receiving inputs of continental sediments via riverine discharges. The principal goal of this study has been to use clay minerals as indicators of sedimentary dynamics in the open shelf system. The distributions of clay mineral in the top layer of the sedimentary cover are shown to be related to their continental sources, but also reflect the influences of winter storms and longshore currents in determining the pathways of sediment transport.The mineralogical composition of the material issuing from the rivers is very similar to the general mineralogical composition of the fine fractions of the seabed sediments. Those deposits that are directly influenced by riverine discharges have higher contents of kaolinite (>20%), whereas those that are not have higher contents of illite (>80%). The available data indicate no significant quantities of terrigenous particles are being discharged from the Spanish rias. Therefore, we conclude that physical processes are controlling the clay mineral distributions and that, despite contributions from the Minho River, the main source of fine detrital particles to the shelf region is the Douro River discharge. These particles settle on the middle shelf, below the 60 m isobath. During storm events these particles are re-suspended and advected northwards to the Galician shelf or into deeper domains. Thus the distributions of the clays indicate there is a net transport of fine sediments both northwards and off-shelf. 相似文献
5.
Phosphorus release from coastal Baltic Sea sediments as estimated from sediment profiles 总被引：1，自引：0，他引：1
We used the decline in total phosphorus (P) concentration with depth in sediment profiles from the North-western Baltic Proper coastal zone to calculate the site-specific amount of sediment P eventually to be released to the water column: The potentially mobile P. P fractionation revealed that iron bound P dominated the potentially mobile P at sites with oxic surface sediment layers. Organic P forms were also a major constituent of the potentially mobile P pool. We determined that 1–7 g P/m2 were potentially mobile at our sites, and the turnover time of this P pool was considered short, i.e., less than a decade. To determine long-term average P fluxes to and from the surface sediment layer, we first multiplied the constant and relatively low P concentration in deeper sediment layers with the sediment accumulation rate to gain the P burial rate. Then the average total P concentration in settling matter was multiplied with the sediment accumulation rate to estimate the depositional P flux at each site. The difference between the depositional and burial rates represents the long-term average release rate of sediment P and varied between 1.0 and 2.7 g P/m2 yr among our sites. These rates are at the same order of magnitude as values reported from other areas of the Baltic Sea, and constitute a major source of P to the water column. 相似文献
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Statistics from Lagrangian observations 总被引：1，自引：0，他引：1
J.H. LaCasce 《Progress in Oceanography》2008,77(1):1-29
We review statistical analyses of Lagrangian data from the ocean. These can be grouped into studies involving single particles and those with pairs or groups of particles. Single particle studies are the most common. The prevalent analysis involves binning velocities geographically to estimate the Eulerian means and lateral diffusivities. However single particle statistics have also been used to study Rossby wave propagation, the influence of bottom topography and eddy heat fluxes. Other studies have used stochastic models to simulate dispersion, calculated Lagrangian frequency spectra and examined the relation between Lagrangian and Eulerian integral scales. Studies involving pairs of particles are fewer, and the results are not well-established yet. There are indications that pair separations grow exponentially in time below the deformation radius, as is also the case in the stratosphere. The behavior at larger scales is less clear, indicating either a turbulent cascade or dispersion by the sheared large-scale circulation. In addition, three or more particles can be used to measure relative vorticity and divergence. 相似文献
8.
D. G. McKnight 《新西兰海洋与淡水研究杂志》2013,47(2):204-213
Prionocidaris australis (Ramsay), Salenocidaris hastigera (A. Agassiz), Echinoneus cyclostomus Leske, Aphanophora echinobrissoides de Meijere (Echinoidea), and Ophiotholia multispina Koehler (Ophiuroidea) are recorded from off Norfolk Island; Peronella hinemoae Mortensen (Echinodea) and a new species of Amphiophiura (Ophiuroidea) are recorded from Wanganella Bank situated about midway between Norfolk Island and northern New Zealand. 相似文献
9.
M. Tiwari R. Ramesh B. L. K. Somayajulu A. J. T. Jull G. S. Burr 《Geo-Marine Letters》2006,26(1):23-30
Rapid shifts in past climate recorded in polar ice sheets have elicited various explanations relating to either thermohaline
circulation changes by ice-rafting or natural greenhouse gas concentrations modulated by climatic conditions in the tropics.
To compare the tropical paleoclimate record with the polar record, one must choose sediment cores from highly productive ocean
regions. Necessarily, such regions reflect the wind records in the tropics, because high productivity is associated with upwelling
driven by winds. Comparing tropical precipitation records with high-latitude records is, however, a more difficult task because
sediments recording paleoprecipitation usually have low sedimentation rates, and offer coarser resolution relative to polar
ice cores. Here, we present δ
18O data of three planktonic species of Foraminifera (a proxy for precipitation) from such a sediment core, spanning the past
35 ka for the equatorial Indian Ocean, which falls under the southwest monsoon (SWM) realm. Results show that minimum SWM
precipitation occurred at the Last Glacial Maximum, with a subsequent increase at Termination IA. During the Holocene, SWM
precipitation intensified uniformly up to the core top (∼2.2 ka b.p.), as revealed by generally decreasing δ
18O values. Variations in precipitation are consistent with climate changes recorded in polar ice sheets. Although the different resolutions of the two records preclude
a rigorous comparison, abrupt cooling/warming events appear to be accompanied by sudden reduction/enhancement in (SWM) rainfall.
Thus, mechanisms with time scales much shorter than a millennium, such as natural greenhouse warming (e.g., CH4 concentration), controlled by emissions from the tropics, could have played a major role in high-latitude climate change. 相似文献
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海藻是海洋生物代谢产物的主要来源之一,能产生丰富多样的生物活性物质.为了更好地利用中国南海的海藻资源,分别对采自中国湛江硇洲岛的1种绿藻基根硬毛藻Chaetomorpha basiretorsa Setchell和4种红藻刺状鱼栖苔Acantophora spicififera (Vahl) Boerg、三列凹顶藻Laurencia tristicha Tseng, Chang et Xia、紫杉状海门冬Asparagopsis taxiformis (Delile) Trevisan、鸡毛菜Pterocladia tenuis Okam进行了生物活性研究,分别对细胞毒活性(KB、Bel-7402、PC-3M、Ketr3和MCF-7)、Na~+,K~+-ATPase抑制活性以及犬血管平滑肌细胞增殖抑制活性进行了筛选,部分海藻提取物表现出一定的生理活性. 相似文献
14.
Kazuyuki Otsuka 《Journal of Oceanography》1986,42(2):106-118
Flow patterns and positions of the Kuroshio in the vicinity of the Izu Ridge are clarified by analyzing hydrographic observations and daily mean sea levels at Hachijo-jima, Miyake-jima and Oshima in the period from 1964 to 1981.Correlations are calculated between differences of dynamic depth anomaly at the surface refered to 1,000 db and differences of daily mean sea level between the two islands. The datum line of the tidal station at Hachijo-jima is about 90 cm higher than that at Miyake-jima, and about 20 cm higher than that at Oshima. A clear correlation is found between the cross-section transport of the Kuroshio and the mean sea-level difference between Hachijo-jima and Miyake-jima. The sea-level difference of the flow pattern without meander off Enshu-nada (type N) tends to be larger than that of the flow patterns with meander (type A and type B). This seems to indicate that the volume transport of the Kuroshio in the meandering period is smaller than that during the straight path period. Large sudden increases or decreases in the mean sea-level difference occur when the flow pattern changes and the Kuroshio axis shifts. The frequency of occurrence of quiet periods in the sea-level difference reflect the flow pattern of the Kuroshio. 相似文献
15.
以采集后适应培养0~24 h以及添加甲烷和硫化钠培养24~240 h的南海冷泉区深海贻贝(Bathymodiolus platifrons)为材料,取其鳃部,分析附生菌的多样性与适应性变化状况。共分离鉴定出贻贝附生菌270株,对菌株的16S r DNA进行聚类分析,结果表明所分离菌株主要分布在4个门,21个属,其中变形菌的数量最多且多样性高。分析发现原位新采集的贻贝鳃部附生菌的多样性较高,6 h后附生菌的多样性明显降低。分别添加甲烷和硫化钠对深海贻贝进行培养,甲烷组与碳代谢有关的假单胞菌的数量逐渐增多,且在甲烷组240 h中发现2株食烷菌属菌株。硫化钠组的芽孢杆菌属所占比例升高。此外还发现4株潜在的新种。本研究实现了深海冷泉区贻贝的实验室培养,并对贻贝鳃部附生菌群结构进行了分析,丰富了海洋极端环境微生物资源库,并为深入解析贻贝与其附生菌之间的相互作用关系奠定了基础。 相似文献
16.
Laboratory incubation of alkenone mixtures with tert-butyl hydroperoxide and di-tert-butyl nitroxide (radical initiator) in hexane, as a means to simulate alkenone autoxidation processes, rapidly led to the formation of allylic hydroperoxides, whose presence was recently demonstrated in Emiliania huxleyi cells. After incubation in seawater and subsequent reduction with NaBH4 (to reduce residual hydroperoxides before analysis), these reaction products quickly disappeared and were replaced by complex mixtures of n-alcohols, fatty acids, alkyldiols and hydroxyacids. Methyl alkenones produced saturated n-alkan-1-ols and fatty acids ranging from C13 to C16 and two series of C13−C16 (ω-1)-hydroxyacids and (1,ω-1)-diols. Ethyl alkenones also afforded C13−C16 saturated n-alkan-1-ols and fatty acids, accompanied by the production of C14−C17 (ω-2)-hydroxyacids and (1,ω-2)-diols. Deuterium labelling allowed us to show that most of the n-alkan-1-ols, hydroxyacids and alkyldiols resulted from the reduction during the NaBH4 treatment of the corresponding aldehydes, ketoxyacids and ketoxyaldehydes formed from heterolytic or homolytic cleavages of allylic hydroperoxyl groups resulting from the oxidation of the double bonds of di- and triunsaturated alkenones. Amongst these products, the (ω-1)- and (ω-2)-hydroxyacids formed after NaBH4 reduction of the (ω-1)- and (ω-2)-ketoxyacids were selected as potential biomarkers for alkenone autoxidation. Re-examination of lipid extracts of post-bloom seawater particulate matter samples from the DYFAMED station in the Ligurian Sea (where strong autoxidative alteration of the lipid distributions had previously been detected) showed the presence of significant amounts of 12-hydroxytetradecanoic, 13-hydroxytetradecanoic, 14-hydroxyhexadecanoic and 15-hydroxyhexadecanoic acids thus providing good evidence that these autoxidative processes occur in natural samples. 相似文献
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Responses of governance systems to change in coastal and marine ecosystems vary from country to country around the globe. Lessons can be learned from country specific case studies, as national governments strive to adapt and respond to issues of concern. This short paper highlights the benefits of a country-specific, special edition of Marine Policy, with a focus on Ireland. Despite the uniqueness of socio-ecological setting, many of the issues faced by policy makers in Ireland, such as the reconciliation of economic development and conservation needs, are shared elsewhere. This special edition was produced at the end of the ‘Celtic Tiger’ in Ireland. As a result, it reflects an era when economic development was very much a priority. The same period represented an unparalleled investment in marine science since the foundation of the State in 1922. Despite this, the papers in the Special Edition point to varying degrees of progress in policy integration and implementation. Papers covering a range of sectors (fisheries, ocean energy, conservation and fisheries) and disciplines (economics, science and management) will be of interest to academics, policy makers, students and practitioners of marine policy. 相似文献
19.
Renewable energy from the ocean 总被引：3，自引：0，他引：3
Growing concern over the threat of global climate change has led to an increased interest in research and development of renewable energy technologies. The ocean provides a vast source of potential energy resources, and as renewable energy technology develops, investment in ocean energy is likely to grow. Research in ocean thermal energy conversion, wave energy, tidal energy, and offshore wind energy has led to promising technologies and in some cases, commercial deployment. These sources have the potential to help alleviate the global climate change threat, but the ocean environment should be protected while these technologies are developed. Renewable energy sources from the ocean may be exploited without harming the marine environment if projects are sited and scaled appropriately and environmental guidelines are followed. 相似文献
20.
Commensal barnacles, Chelonibia testudinaria, from logger-head turtles have 18O and 13C variations in their calcitic shells that record the environments in which the turtles live. Isotopic profiles from the barnacle shells can thus be interpreted to reconstruct movements of the host turtle between open ocean and brackish-water regimes. 相似文献